Remarkable Salinity Tolerance of Seven Species of Naked Amoebae (gymnamoebae)

The salinity tolerance of naked amoebae collected from sites ranging from ca. 0‰ to 160‰ were compared in laboratory experiments. Amoebae were collected from hypersaline ponds around the perimeter of the Salton Sea, California, where salinities averaged 160‰, and directly from the shoreline waters of the Sea where salinities were generally between 44 and 48‰. Naked amoebae were also collected from the intertidal zone of a Florida beach, a habitat subject (on occasion) to salinity fluctuations within the range 6–85‰. From these combined sites, 6 clones of amoebae were isolated for salinity tolerance experiments (2 marine beach isolates, 2 Salton Sea isolates, and 2 hypersaline pond isolates). A seventh clone, Acanthamoeba polyphaga, a common freshwater/soil amoeba, was obtained from a Culture Collection. Laboratory experiments compared the effects of gradually changing culture salinity versus no salinity acclimatization. Growth rate and culture yield were used as indices of effect. Generally, amoebae were tolerant over a wide range of salinity conditions (in terms of growth and yield) and were not markedly influenced by pre-conditioning to salinity changes throughout the experiments. Overall, the freshwater amoeba Acanthamoeba grew between 0 and 12‰, the marine clones grew in the range of 2–120‰, and the Salton Sea clones reproduced between 0 and 138 ‰. The hypersaline clones were the most resilient and grew between 0 and 270‰ salt. The survival and activity of large populations of naked amoebae in sites subject to salinity fluctuations suggest that they should be considered in future studies to better understand their, as yet, undefined ecological role.     

Matching molecular diversity and ecophysiology of benthic cyanobacteria and diatoms in communities along a salinity gradient

The phylogenetic diversity of oxygenic phototrophic microorganisms in hypersaline microbial mats and their distribution along a salinity gradient were investigated and compared with the halotolerances of closely related cultivated strains. Segments of 16S rRNA genes from cyanobacteria and diatom plastids were retrieved from mat samples by DNA extraction and polymerase chain reaction (PCR), and subsequently analysed by denaturing gradient gel electrophoresis (DGGE). Sequence analyses of DNA from individual DGGE bands suggested that the majority of these organisms was related to cultivated strains at levels that had previously been demonstrated to correlate with characteristic salinity responses. Proportional abundances of amplified 16S rRNA gene segments from phylogenetic groupings of cyanobacteria and diatoms were estimated by image analysis of DGGE gels and were generally found to correspond to abundances of the respective morphotypes determined by microscopic analyses. The results indicated that diatoms accounted for low proportions of cells throughout, that the cyanobacterium Microcoleus chthonoplastes and close relatives dominated the communities up to a salinity of 11% and that, at a salinity of 14%, the most abundant cyanobacteria were related to highly halotolerant cultivated cyanobacteria, such as the recently established phylogenetic clusters of Euhalothece and Halospirulina . Although these organisms in cultures had previously demonstrated their ability to grow with close to optimal rates over a wide range of salinities, their occurrence in the field was restricted to the highest salinities investigated.     

Anammox bacterial populations in deep marine hypersaline gradient systems

To extend the knowledge of anaerobic ammonium oxidation (anammox) habitats, bacterial communities were examined in two hypersaline sulphidic basins in Eastern Mediterranean Sea. The 2 m thick seawater–brine haloclines of the deep anoxic hypersaline basins Bannock and L’Atalante were sampled in intervals of 10 cm with increasing salinity. ¹⁵N isotope pairing incubation experiments showed the production of ²⁹N₂ and ³⁰N₂ gases in the chemoclines, ranging from 6.0 to 9.2 % salinity of the L’Atalante basin. Potential anammox rates ranged from 2.52 to 49.65 nmol N₂ L^?1 day^?1 while denitrification was a major N₂ production pathway, accounting for more than 85.5 % of total N₂ production. Anammox-related 16S rRNA genes were detected along the L’Atalante and Bannock haloclines up to 24 % salinity, and the amplification of the hydrazine synthase genes (hzsA) further confirmed the presence of anammox bacteria in Bannock. Fluorescence in situ hybridisation and sequence analysis of 16S rRNA genes identified representatives of the marine anammox genus ‘Candidatus Scalindua’ and putatively new operational taxonomic units closely affiliated to sequences retrieved in marine environments that have documented anammox activity. ‘Scalindua brodae’ like sequences constituted up to 84.4 % of the sequences retrieved from Bannock. The anammox community in L’Atalante was different than in Bannock and was stratified according to salinity increase. This study putatively extends anammox bacterial habitats to extremely saline sulphidic ecosystems.     

Oil-bioremediation potential of two hydrocarbonoclastic, diazotrophic Marinobacter strains from hypersaline areas along the Arabian Gulf coasts

Two halophilic, hydrocarbonoclastics bacteria, Marinobacter sedimentarum and M. flavimaris, with diazotrophic potential occured in hypersaline waters and soils in southern and northern coasts of Kuwait. Their numbers were in the magnitude of 10³ colony forming units g^?1. The ambient salinity in the hypersaline environments was between 3.2 and 3.5 M NaCl. The partial 16S rRNA gene sequences of the two strains showed, respectively, 99 and 100 % similarities to the sequences in the GenBank. The two strains failed to grow in the absence of NaCl, exhibited best growth and hydrocarbon biodegradation in the presence of 1 to 1.5 M NaCl, and still grew and maintained their hydrocarbonoclastic activity at salinities up to 5 M NaCl. Both species utilized Tween 80, a wide range of individual aliphatic hydrocarbons (C₉–C₄₀) and the aromatics benzene, biphenyl, phenanthrene, anthracene and naphthalene as sole sources of carbon and energy. Experimental evidence was provided for their nitrogen-fixation potential. The two halophilic Marinobacter strains successfully mineralized crude oil in nutrient media as well as in hypersaline soil and water microcosms without the use of any nitrogen fertilizers.     

Bacterial chitin utilization at halophilic conditions

Chitin is a dominant structural polymer produced in large amounts by brine shrimp Artemia in hypersaline lakes. Microbiological analysis of chitin utilization as a growth substrate in hypersaline chloride–sulfate lakes in the south Kulunda Steppe (Altai, Russia) revealed two groups of bacteria able to grow on chitin at moderate salinity. Under aerobic conditions, an enrichment culture was obtained at 2 M NaCl. Further purification resulted in the isolation of strains HCh1 and strain HCh2, identified as representatives of the genera Saccharospirillum and Arhodomonas (both in the Gammaproteobacteria). The chitin-utilizing potential has not been previously recognized in these genera. The Saccharospirillum sp. strain HCh1 grew on chitin within the salinity range from 0.5 to 3.25 M NaCl (optimum at 1 M), while Arhodomonas sp. strain HCh2 grew up to 2.5 M NaCl but had a higher salt optimum at 1.5 M. Anaerobic enrichments grew with chitin at 2 and 4 M NaCl, but growth in the latter was extremely slow and the culture eventually lost viability. The enrichment at 2 M NaCl resulted in the isolation of strain HCh-An1, identified as a distant new species of the genus Orenia in the clostridial order Halanaerobiales. It was able to grow on chitin within a salinity range from 1.0 to 2.5 M NaCl (optimum at 1.5 M). The strain is proposed as a new species of the genus Orenia—O. chitinitropha.     

Microbial mats and physicochemistry in a saltern in the Bretagne (France) and in a laboratory scale saltern model

Abstract A saltern near La Baule (Bretagne, France) was remodeled in a programmable temperature and humidity controlled walk-in environmental chamber resembling the characteristics of the original saltern. The saltern showed different types of microbial mats predominantly composed of algae, oxy- and anoxyphotobacteria, and associated chemoorganotrophic bacteria, fungi and animals. Well-developed microbial mats were found up to a salinity of 10% during the three or four months in summer when salinity gradients and NaCl precipitation were established. The main phototrophic organisms were diatoms, the cyanobacteria Aphanothece, Microcoleus, Spirulina , and Oscillatoria , and Chromatiaceae. At higher salinity, Halobacterium sp., diatoms, and Dunaliella were dominant. Typical microbial mats and saltern-typical invertebrate, algal and bacterial species also developed in the saltern model, building up a stable community. The ionic composition of the brines and physicochemical parameters were similar to those determined for the original saltern. Different photosynthetic organisms, e.g. a filamentous purple bacterium and a hypersaline Chloroflexus -like organism, could be enriched within the microbial mats by changing the light regime.     

SALINITY TOLERANCE OF DIATOMS FROM THALASSIC HYPERSALINE ENVIRONMENTS

Thirty-four benthic diatom strains were isolated from thalassic hypersaline marine environments and their salinity tolerance characterized in growth experiments conducted at salinities ranging from 0.5% to 17.5% (weight of total salts per volume, g·100 mL ^{− 1}). The results were compared with the patterns of diatom species distribution and abundance in hypersaline evaporation ponds and tidal channels of Guerrero Negro, Baja California Sur, Mexico. The isolated strains were representative of the diatom assemblages present in the saltern ponds but were less so of natural assemblages in tidal channels. In general, we found a clear decreasing trend of diatom diversity in the field and in the isolated strains with increasing salinity. With some exceptions, the upper limit of salinity tolerance in cultivated strains corresponded to their distribution in field samples. However, the relative abundance of species in the field was not correlated with growth rates achieved in culture for the same salinities. Most cultured strains exhibited extreme euryhalinity growing well from brackish to hypersaline conditions, but the particulars of salt tolerance were quite diverse among strains. The most halotolerant taxa, two Amphora species, Amphora cf. subacutiuscula Schoeman, Nitzschia fusiformis Grunow, and Entomoneis sp., grew well in salinities ranging from 0.5% to 15%. Three strains of Pleurosigma strigosum W. Smith that were unable to grow in salinities less than 5% total salts represent the only true halophilic diatoms ever reported. The fact that many strains displayed a remarkable halotolerance, with optimal or near-optimal growth rates at salinities as high as three times that of seawater, implies that diatoms from hypersaline environments are evolutionarily highly adapted to such environments.     

Amino acid signatures of salinity on an environmental scale with a focus on the Dead Sea

The increase of the acidic nature of proteins as an adaptation to hypersalinity has been well documented within halophile isolates. Here we explore the effect of salinity on amino acid preference on an environmental scale. Via pyrosequencing, we have obtained two distinct metagenomic data sets from the Dead Sea, one from a 1992 archaeal bloom and one from the modern Dead Sea. Our data, along with metagenomes from environments representing a range of salinities, show a strong linear correlation (R² = 0.97) between the salinity of an environment and the ratio of acidic to basic amino acids encoded by its inhabitants. Using the amino acid composition of putative protein‐encoding reads and the results of 16S rRNA amplicon sequencing, we differentiate recovered sequences representing microorganisms indigenous to the Dead Sea from lateral gene transfer events and foreign DNA. Our methods demonstrate lateral gene transfer events between a halophilic archaeon and relatives of the thermophilic bacterial genus Thermotoga and suggest the presence of indigenous Dead Sea representatives from 10 traditionally non‐hyperhalophilic bacterial lineages. The work suggests the possibility that amino acid bias of hypersaline environments might be preservable in fossil DNA or fossil amino acids, serving as a proxy for the salinity of an ancient environment. Finally, both the amino acid profile of the 2007 Dead Sea metagenome and the V9 amplicon library support the conclusion that the dominant microorganism inhabiting the Dead Sea is most closely related to a thus far uncultured relative of an alkaliphilic haloarchaeon.     

The role of glycerol in the nutrition of halophilic archaeal communities: a study of respiratory electron transport

Abstract Respiratory electron transport activity in the Dead Sea and saltern crystallizer ponds, hypersaline environments inhabited by dense communities of halophilic archaea and unicellular green algae of the genus Dunaliella , was assayed by measuring reduction of 2-( p -iodophenyl)-3( p -nitrophenyl)-5-phenyl tetrazolium chloride (INT) to INT-formazan. Typical rates obtained were in the order of 5.5–17.7 nmol INT reduced h ⁻¹ per 10⁶ cells at 35 ° C. In Dead Sea water samples, respiratory activity was stimulated more than two-fold by addition of glycerol, but not by any of the other carbon compounds tested, including sugars, organic acids, and amino acids, or by addition of inorganic nutrients. Stimulation by glycerol had a half-saturation constant of 0.75 μM. A similar respiratory activity was also found when Dead Sea water samples were diluted with distilled water and incubated in the light. As Dunaliella cells did not reduce INT, it is suggested that photosynthetically produced glycerol leaking from the algae is the preferred carbon and energy source for the development of halophilic archaea in hypersaline environments. In samples from saltern crystallizer pond stimulation of INT reduction by glycerol was much less pronounced, probably because the community was less severely carbon-limited.     

Fungal life in the extremely hypersaline water of the Dead Sea: first records.

The first report, to our knowledge, on the occurrence of filamentous fungi in the hypersaline (340 g salt l-1) Dead Sea is presented. Three species of filamentous fungi from surface water samples of the Dead Sea were isolated: Gymnascella marismortui (Ascomycota), which is described as a new species, Ulocladium chlamydosporum and Penicillium westlingii (Deuteromycota). G. marismortui and U. chlamydosporum grew on media containing up to 50% Dead Sea water. G. marismortui was found to be an obligate halophile growing optimally in the presence of 0.5-2 M NaCl or 10 30% (by volume) of Dead Sea water. Isolated cultures did not grow on agar media without salt, but grew on agar prepared with up to 50% Dead Sea water. This suggests that they may be adapted to life in the extremely stressful hypersaline Dead Sea.     

Polyphasic characterization of benthic, moderately halophilic, moderately thermophilic cyanobacteria with very thin trichomes and the proposal of Halomicronema excentricum gen. nov., sp. nov.

A new genus of moderately halophilic, moderately halotolerant and moderately thermophilic cyanobacteria with very thin trichomes is described. The four strains included in this genus were isolated from benthic microbial mats in a man-made hypersaline pond. Trichomes were around 1 microm thick, with small constrictions at the cross-walls and diffluent colorless sheaths. Thylakoids were parallel to the cell wall, but thylakoids and nucleoid were often excentrically arranged within the cytoplasm with respect to the main trichome axis. Strains grew at between 3.2 and 12-15% (w/v) salinity with optima between 3.2 and 12%. They showed lower temperature limits around 20 degrees C and upper limits between 45 and 50 degrees C, with optima between 28 and 45-50 degrees C. Carotenoid and mycosporine amino-acid complements were identical among strains. Phylogenetic analyses based on 16S rRNA gene sequence showed that all strains were closely related (99% or higher similarity) and distantly related to other cyanobacteria (91% or lower similarity). We propose the new genus and species Halomicronema excentricum for these strains. The type strain is TFEP1.     

GROWTH AND ORGANIC OSMOLYTES OF GEOGRAPHICALLY DIFFERENT ISOLATES OF MICROCOLEUS CHTHONOPLASTES (CYANOBACTERIA) FROM BENTHIC MICROBIAL MATS:RESPONSE TO SALINITY CHANGE1

The comparative growth and osmotic acclimation often culture strains of the marine benthic cyanobacterium Microcoleus chthonoplastes Thuret isolated from microbial mats in Germany, Spain, Egypt, the United States, Mexico, Chile, and Australia were investigated in salinities ranging from freshwater to twice seawater. All isolates showed a broad growth versus salinity response consistent with the dominance of this species in intertidal and hypersaline microbial communities. Growth optima, salinity preferences, and maximum growth rates differed for each isolate and could be related to the habitat from which they were isolated. This is most obvious when comparing strains from brackish habitats with those from a hypersaline lake. While the former isolates exhibited sharply pronounced growth optima under hyposaline conditions, cultures from the hypersaline environment grew best in salinity more than double seawater. The major low-molecular weight organic compounds present in all M. chthonoplastes strains were the carbohydrates glycosylglycerol and trehalose. This was proven by using ¹³C-nuclear magnetic resonance spectroscopy. Glycosylglycerol was synthesized and accumulated with increasing salinities, indicating its role as an osmolyte. In contrast, trehalose was present in relatively high concentrations under hyposaline conditions only. Differences in the patterns of growth versus salinity, as well as in those of osmotic acclimation among the M. chthonoplastes isolates, point to the development of different physiological ecotypes within the species.     

ALGAL COMMUNITY DYNAMICS AND HALOTOLERANCE IN A TERRESTRIAL,HYPERSALINE ENVIRONMENT1

We studied the algal community of the Great Salt Plains (GSP), an expansive (65 km²) salt flat situated in north‐central Oklahoma, USA that has been designated as the Salt Plains Microbial Observatory (SPMO) by the National Science Foundation. The GSP offered a unique opportunity to study a terrestrial, hypersaline algal community that experiences wide‐ranging environmental conditions. We were able to show that ammonium‐N, rather than salinity, was the most important predictor of total algal biomass. However, salinity was found to be a significant controlling variable in diatom distribution at the GSP, where diatom abundance was negatively correlated with porewater salinity concentrations. Overall, chlorophytes (likely dominated by Dunaliella spp.) were the most abundant algal group at the consistently hypersaline (>300 ppt) south site. Diatom and cyanobacterial biomass were on average highest at the central site, which experienced greater fluctuations in salinity. While taxonomic diversity was limited to three algal groups (chlorophytes, diatoms, and cyanobacteria), the salinity preferences and halotolerance ranges of isolated strains were quite variable. Although porewater salinities at the GSP are commonly near saturation (>300 ppt), the large majority of isolates had halotolerance ranges below 150 ppt. This suggests that algae at the GSP rarely achieve maximum growth rates, and could only do so when intermittent rain events reduce salinity to optimal levels. Because the vast majority of our strains were isolated from salt‐saturated soil samples, maintaining viability (rather than growth efficiency) appears to be the most successful adaptation to the extreme conditions at the GSP.     

Effect of salinity on filtration rates of mussels Mytilus edulis with special emphasis on dwarfed mussels from the low-saline Central Baltic Sea

The effect of salinity on the filtration rate of blue mussels, Mytilus edulis, from the brackish Great Belt (Denmark) and the low-saline Central Baltic Sea, respectively, was studied. First, we measured the effect of long-term (weeks) constant ambient salinities between 5 and 30 psu on the filtration rate of M. edulis collected in the Great Belt where the mean salinity is 17 psu. At salinities between 10 and 30 psu, the filtration rates did not vary much, but at 5 psu the filtration rates were significantly lower. Next, we studied dwarfed M. edulis (<25 mm shell length) from Central Baltic Sea (Askö, Sweden) where the mean salinity is 6.5 psu. The maximum filtration rate (F, ml min^?1 ind.^?1) as a function of shell length (L, mm) and dry weight of soft parts (W, mg) were found to be: F = 0.003L ^2.71 and F = 0.478W ^0.92, respectively, and these results indicate that the filtration rates of dwarfed Baltic Sea mussels are comparable to filtration rates of Great Belt mussels of similar size exposed to salinities >10 psu. When Baltic Sea mussels acclimatized to 20 psu in the laboratory were exposed to 6.5 psu this caused a drastic reduction in the filtration rate, but after about 2 days the previous high filtration rate was regained at 6.5 psu, and further, a similar pattern was observed when the 6.5 psu exposed mussels were finally re-exposed to 20 psu. The observed lack of Great Belt mussels to completely adjust to 5 psu, in contrast to the ease of Baltic Sea mussels to adjust back and forth between 6.5 and 20 psu, is remarkable and may perhaps be explained by different genotypes of Great Belt and Baltic Sea mussels.     

Halotaxis of cyanobacteria in an intertidal hypersaline microbial mat

An intertidal hypersaline cyanobacterial mat from Abu Dhabi (United Arab Emirates) exhibited a reversible change in its surface colour within several hours upon changes in salinity of the overlying water. The mat surface was orange‐reddish at salinities above 15% and turned dark green at lower salinities. We investigated this phenomenon using a polyphasic approach that included denaturing gradient gel electrophoresis, microscopy, high‐performance liquid chromatography, hyperspectral imaging, absorption spectroscopy, oxygen microsensor measurements and modelling of salinity dynamics. Filaments of Microcoleus chthonoplastes, identified based on 16S rRNA sequencing and morphology, were found to migrate up and down when salinity was decreased below or increased above 15%, respectively, causing the colour change of the mat uppermost layer. Migration occurred in light and in the dark, and could be induced by different salts, not only NaCl. The influence of salinity‐dependent and independent physico‐chemical parameters, such as water activity, oxygen solubility, H₂S, gravity and light, was excluded, indicating that the observed migration was due to a direct response to salt stress. We propose to term this salinity‐driven cyanobacterial migration as ‘halotaxis’, a process that might play a vital role in the survival of cyanobacteria in environments exposed to continuous salinity fluctuations such as intertidal flats.     

Benthic diatoms in the salinas of the Dry Creek saltfields,South Australia

Given that diatom assemblages are a well-recognised method of characterising the water quality in freshwater streams, it seems reasonable to investigate its applicability to solar saltfields. A summer collection of benthic diatoms was undertaken in the salinas of the Dry Creek solar saltfields in South Australia for this purpose. The facility inputs seawater both from a low nutrient samphire creek and poorer quality, high nutrient samphire creek. Salinity and nutrient status of the pools and concentrating salinas have been thoroughly characterized over many years. The addition of JJ periphytometers to the sampling regime in the summer of 2001–2002 allowed the collection of benthic diatoms from these sites. Of the 69 species collected during the study, 16 species occurred only in oligotrophic waters with salinities less than 70 g/l TDS (total dissolved solids). Twenty species of diatoms occurred only in the eutrophic waters with salinities less than 70 g/l TDS, eight species were restricted to the hypersaline ponds and the remainder were undiscriminating in their ecological preferences. Guest Editor: John M. Melack Saline Water and their Biota     

Microbial and chemical characterization of underwater fresh water springs in the Dead Sea

Due to its extreme salinity and high Mg concentration the Dead Sea is characterized by a very low density of cells most of which are Archaea. We discovered several underwater fresh to brackish water springs in the Dead Sea harboring dense microbial communities. We provide the first characterization of these communities, discuss their possible origin, hydrochemical environment, energetic resources and the putative biogeochemical pathways they are mediating. Pyrosequencing of the 16S rRNA gene and community fingerprinting methods showed that the spring community originates from the Dead Sea sediments and not from the aquifer. Furthermore, it suggested that there is a dense Archaeal community in the shoreline pore water of the lake. Sequences of bacterial sulfate reducers, nitrifiers iron oxidizers and iron reducers were identified as well. Analysis of white and green biofilms suggested that sulfide oxidation through chemolitotrophy and phototrophy is highly significant. Hyperspectral analysis showed a tight association between abundant green sulfur bacteria and cyanobacteria in the green biofilms. Together, our findings show that the Dead Sea floor harbors diverse microbial communities, part of which is not known from other hypersaline environments. Analysis of the water's chemistry shows evidence of microbial activity along the path and suggests that the springs supply nitrogen, phosphorus and organic matter to the microbial communities in the Dead Sea. The underwater springs are a newly recognized water source for the Dead Sea. Their input of microorganisms and nutrients needs to be considered in the assessment of possible impact of dilution events of the lake surface waters, such as those that will occur in the future due to the intended establishment of the Red Sea-Dead Sea water conduit.     

Environmental salinity-modified osmoregulatory response in the sub-Antarctic notothenioid fish Eleginops maclovinus

In this study we assessed changes in the osmoregulatory system of juvenile sub-Antarctic Eleginops maclovinus submitted to different environmental salinities (5, 15, 32 and 45 psu) using two different acclimation trials: (1) an end-point experiment (exposure for 14 days) and (2) a time course experiment (specimens were sampled on days 1, 3, 7 and 14 post-transfer). Plasma osmolality, cortisol and metabolites (glucose, lactate and protein) values as well as Na⁺, K⁺-ATPase (NKA) activity were assessed in several osmoregulatory tissues (gills, kidney and intestine). In both trials, acclimation to different environmental salinities for 14 days induced changes in plasma metabolites (glucose, lactate and proteins) as well as cortisol values related to salinity challenges. Plasma osmolality and gill NKA activity presented a direct and positive relationship with respect to environmental salinity, while kidney NKA activity showed a “U-shaped” relationship. Anterior intestinal NKA activity increased in response to environmental salinity and apparently did not change in the middle portion of this organ, while it was enhanced in the posterior portion in environmental salinities different than seawater. Plasma metabolite values increased under hypo- and hypersaline conditions, indicating the importance of these energy substrates in extreme environments. The time course study revealed that specimens of E. maclovinus are able to accommodate their osmotic and metabolic system to respond to osmoregulatory challenges by allostatic changes.     

The distribution and abundance of algae in saline lakes of Saskatchewan,Canada

Collections of algae, mainly planktonic, were made from 41 saline lakes in southern Saskatchewan ranging in salinity from 3.2 to 428 g l^-1. Algae in 7 phyla, 8 classes, 42 families, 91 genera and 212 species and varieties were identified. Fourteen species were restricted to hypersaline (50 g l^-1) waters and eleven of these were diatoms. In general, species diversity was inversely related to lake salinity. Algae that were important community constituents over a broad spectrum of salinities were the green algae Ctenocladus circinnatus, Dunaliella salina and Rhizoclonium hieroglyphicum, the blue-green Lyngbya Birgei, Microcystis aeruginosa, Oscillatoria tenuis, O. Utermoehli and Nodularia spumigena and the diatoms Melosira granulata, Stephanodiscus niagarae and Chaetoceros Elmorei. In general green algae were dominant when lake salinity exceeded 100 g l^-1 although diatoms played important roles in most of these highly saline lakes except for Patience Lake.